Abstract Details
(2020) Clay Minerals and the Ancient Martian Carbon Cycle
Bristow T, Rampe E, Vaniman D, Blake D, Sutter B & Grotzinger J
https://doi.org/10.46427/gold2020.262
01b: Room 1, Monday 22nd June 23:30 - 23:33
Thomas Bristow
View all 2 abstracts at Goldschmidt2020
View abstracts at 8 conferences in series
Elizabeth Rampe View all 3 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
David Vaniman View all 2 abstracts at Goldschmidt2020 View abstracts at 4 conferences in series
David Blake View all 2 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Brad Sutter View abstracts at 3 conferences in series
John Grotzinger View abstracts at 15 conferences in series
Elizabeth Rampe View all 3 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
David Vaniman View all 2 abstracts at Goldschmidt2020 View abstracts at 4 conferences in series
David Blake View all 2 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Brad Sutter View abstracts at 3 conferences in series
John Grotzinger View abstracts at 15 conferences in series
Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.
Submitted by Jon Zaloumis on Monday 15th June 22:26
The siderite and talc detections are very interesting. Do they correspond to veins or other alteration textures?
The siderite and talc detections are very interesting. Do they correspond to veins or other alteration textures?
Submitted by Jon Zaloumis on Monday 15th June 22:26
The siderite and talc detections are very interesting. Do they correspond to veins or other alteration textures?
The siderite and talc detections are very interesting. Do they correspond to veins or other alteration textures?
Submitted by Jeffrey Catalano on Saturday 20th June 20:11
When do you think iron oxidized in the GT unit, during deposition/initial alteration, or at a later time? Siderite, hematite, and Fe(III)-rich smectites cannot form together, they require different redox conditions.
When do you think iron oxidized in the GT unit, during deposition/initial alteration, or at a later time? Siderite, hematite, and Fe(III)-rich smectites cannot form together, they require different redox conditions.
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